Ionic diffusion coefficients are
important parameters to model
mass transport processes in many high temperature water systems, such
as nuclear and fossil-fueled power stations and hydrothermal geochemical
systems. This work is a critical assessment of the molar conductivity
data for aqueous potassium chloride which is directly related to diffusion
coefficients. The literature includes more than 550 experimental data
sets measured from temperatures T = 273 to 1073 K,
pressures p = 0.1 to 1200 MPa, and water densities
ρw = 85 to 1000 kg·m–3. In
some cases, the measurements were reanalyzed with modern conductivity
equations to yield more accurate limiting molar conductivity data,
Λ°KCl. The selected Λ°KCl data were split into single-ion conductivities (λ°) for
K+ and Cl– using transference number
extrapolations. Simple empirical functions of the solvent viscosity
and density were derived that can reproduce the data from T = 288 to 923.15 K, p = 0.1 to 407 MPa,
and ρw = 450 to 1000 kg·m–3 to less than the estimated uncertainties. A revised equation to
express the temperature and density dependence of KCl ion-pair formation
constant, K
A, based on flow conductivity
measurements (T = 491 to 873 K, p = 2.25 to 300 MPa, and ρw = 160 to 852.45 kg·m–3), is also reported. This study recommends the use
of potassium chloride as a chemical standard for high temperature
conductivity experiments along with the Fuoss–Hsia–Fernández–Prini
(FHFP) equation and the fitted parameters for Λ°KCl and K
A reported here to verify the accuracy
of hydrothermal conductivity measurements.